Search results for "Interrill flow"

showing 3 items of 3 documents

Roughness effect on the correction factor of surface velocity for rill flows

2021

Flow velocity is one of the most important hydrodynamic variables for both channelized (rill and gullies) and interrill erosive phenomena. The dye tracer technique to measure surface flow velocity Vs is based on the measurement of the travel time of a tracer needed to cover a known distance. The measured Vs must be corrected to obtain the mean flow velocity V using a factor αv = V/Vs which is generally empirically deduced. The Vs measurement can be influenced by the method applied to time the travel of the dye-tracer and αv can vary in different flow conditions. Experiments were performed by a fixed bed small flume simulating a rill channel for two roughness conditions (sieved soil, gravel)…

Roughness effectgeographysoil erosiongeography.geographical_feature_categoryrill flowSoil scienceSurface velocitycorrection factorflow velocityRilldye methodFlow velocitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliinterrill flowGeologyWater Science and TechnologyHydrological Processes
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Dye-tracer technique for rill flows by velocity profile measurements

2020

Abstract Water flow on hillslope soil surface supplies energy which is required to detach soil particles, to transport and deposit sediments, therefore flow velocity is a key variable related to hillslope hydrodinamics of soil erosion processes. Among the different methods available for measuring velocity of shallow interrill and rill flow, the trace technique is widely used. Trace technique is applied by adding a material (salt, magnetic material, water isotope, floating object) and then measuring the speed of the material to travel a known distance from the injection point. When flow velocity is measured using a dye-tracing method, the mean velocity is calculated by multiplying the measur…

Correction factorDye method010504 meteorology & atmospheric sciencesWater flowFlow (psychology)Surface finish01 natural sciencesPhysics::GeophysicsPhysics::Fluid DynamicsFlow velocitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorySediment04 agricultural and veterinary sciencesMechanicsPlumeRillFlumeFlow velocityRill flowSoil erosion040103 agronomy & agriculture0401 agriculture forestry and fisheriesInterrill flowGeologyCATENA
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Flume experiments for assessing the dye-tracing technique in rill flows

2021

Abstract Flow velocity controls hillslope soil erosion and is a key hydrodynamic variable involved in sediment transport and deposition processes. The dye-tracer technique is one of the most applied methods for measuring velocity of shallow interrill and rill flow. The technique is based on the injection of a tracer in a specific point and the measurement of its speed to travel the known distance from the injection point to a given channel section. The dye-tracer technique requires that the measured surface flow velocity has to be corrected to obtain the mean flow velocity using a correction factor which is generally empirically deduced. The technique has two sources of uncertainties: i) th…

Correction factorDye methodFlow (psychology)0207 environmental engineering02 engineering and technology01 natural sciences010309 opticssymbols.namesakeFlow velocity0103 physical sciencesFroude numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliElectrical and Electronic Engineering020701 environmental engineeringInstrumentationgeographygeography.geographical_feature_categoryDye tracingReynolds numberMechanicsComputer Science ApplicationsFlumeRillFlow conditionsFlow velocityModeling and SimulationRill flowSoil erosionsymbolsInterrill flowGeologyFlow Measurement and Instrumentation
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